Showing posts with label Space. Show all posts
Showing posts with label Space. Show all posts

Sun Eruption Supercharges Northern Lights


Sun Eruption Supercharges Northern Lights Displays This Weekend - A massive eruption on the sun Friday (March 15) unleashed a wave of intense solar particles at Earth that may spark a geomagnetic storm and boost weekend aurora displays.

The Earth-directed solar storm occurred Friday at 2:54 a.m. EDT (0654 GMT) in what astronomers call a coronal mass ejection — or CME — a sun eruption that can release billions of tons of solar material into space. The particles typically take between one and three days to reach Earth, where they can pose a hazard to satellites and electronic systems in orbit and on the planet's surface, NASA officials said in a statement.

The solar particles from the Friday eruption were expected to reach Earth today (March 17).

The ESA and NASA Solar Heliospheric Observatory (SOHO) captured these images of the sun spitting out a coronal mass ejection (CME) on March 15, 2013, from 3:24 to 4:00 a.m. EDT.

"High-latitude and possibly even middle-latitude sky watchers should be alert for auroras this weekend," the website Spaceweather.com, which tracks space weather and stargazing events, said in a weekend alert. 

The Friday sun eruption sent a wave of solar particles streaking toward Earth at about 900 miles per second, according to observations by NASA and European spacecraft. That is the equivalent of a mind-boggling about 3.2 million miles per hour (5.2 million km/h).

According to NASA, this "is a fairly fast speed for CMEs. Historically, CMEs at this speed have caused mild to moderate effects at Earth."

The solar eruption should not pose a threat to satellites and spacecraft around Earth, but it may pass NASA's Messenger spacecraft orbiting Mercury and the infrared Spitzer Space Telescope, agency officials said. NASA alerted the mission operation centers for both missions.

"There is, however, only minor particle radiation associated with this event, which is what would normally concern operators of interplanetary spacecraft since the particles can trip on board computer electronics," NASA officials said.

An alert by the Space Weather Prediction Center operated by the National Oceanic and Atmospheric Administration reported that the Earth's geomagnetic field could be at "unsettled to major storm levels" once the CME particles reached Earth Sunday. There was a 70 percent chance of a geomagnetic storm today, the Spaceweather.com alert added.

When the sun fires off an eruption in Earth's direction, the charged solar particles that reach the planet are funneled to the Earth's poles by its magnetic field. When the particles interact with the Earth's atmosphere, they can cause a glow visible from the ground: the northern lights.

Northern lights displays over the North Pole region are known as the aurora borealis. Their southern counterpart is known as the aurora australis.

The sun is currently in the midst of an active phase of its 11-year solar weather cycle and is expected to reach its peak activity in 2013. ( space.com )

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Giant Alien Planet in Supersized Solar System May Solve Mystery


Giant Alien Planet in Supersized Solar System May Solve Mystery - The glowing atmosphere of a strangely giant alien world could help solve mysteries of not just how it formed, but how our own solar system arose, scientists say.

The exoplanet discovery comes from the most detailed look yet at the alien planets around the distant star HR 8799, which lies about 130 light-years from Earth. The HR 8799 system is home to four giant planets orbiting a relatively young, 30-million-year-old star, with each planet far larger than any world found in Earth's solar system.

The planets orbiting HR 8799 weigh in at between five to 10 times the mass of Jupiter and are still glowing with the heat of their formation, allowing researchers to directly image them.

"It's the only system in which multiple planets can individually be seen," said study co-author Bruce Macintosh, an astronomer at Lawrence Livermore National Laboratory in California.

This artist's rendering of the planetary system of HR 8799 130 light-years from Earth as it may have appeared at an early stage in its evolution. The image shows the giant exoplanet HR 8799c, as well as a disk of gas and dust, and interior plan 

One of the discovery images of the supersized alien solar system around the star HR 8799, about 130 light-years from Earth, obtained by the Keck II telescope using an adaptive optics system and NIRC2 Near-Infrared Imager. The rectangle indicate
The planetary system resembles a scaled-up version of our solar system, suggesting there may be smaller Earth-size planets closer in, although the researchers currently have not yet seen any.

It even "has something that kind of looks like maybe an asteroid belt interior to the closest giant planet like we have in our solar system, and something that maybe you can refer to as an Oort cloud analog out beyond the most distant gas giant" — that is, a cloud of icy comets, said study lead author Quinn Konopacky, an astronomer at the University of Toronto. 

Exoplanet's atmosphere revealed

The astronomers concentrated on one of the star's visible planets, named HR 8799c, a colossal gas giant about seven times the mass of Jupiter. It circles the star HR 8799 at a range comparable to Pluto's distance from the sun.

The birth of such a massive planet at such a great distance from its parent star conflicts with the two popular models of planetary formation. In the multistep process known as core accretion, gas slowly accumulates onto a planetary core, while the mechanism known as gravitational instability involves the simultaneous creation of a planet's interior and atmosphere.

"In the traditional core accretion model of planet formation, it is difficult to form planets as large as the HR 8799 planets at such large distances from their parent star," Konopacky told SPACE.com. "Typically, in this model, objects the size of Jupiter or larger must form much closer to their parent star. This is for several reasons, but has a lot to do with there being less material at large distances from the star that can form planets."

"In the gravitational instability method of formation, it is possible to form big planets at large distances, usually because they invoke a much more massive disc of material," Konopacky added. "But the model generally predicts that there should be many more massive objects orbiting lots of other stars at these distances, and these kinds of objects have not been discovered in surveys [of many stars for exoplanets]."

To help solve this mystery, the scientists analyzed the glow from HR 8799c using a high-resolution imaging spectrograph called OSIRIS at the Keck Observatory in Hawaii. Molecules in atmospheres can absorb light, resulting in patterns known as spectra that allow scientists to identify what they are.

HR8799c is both fairly bright and located a fair distance from its star, helping the researchers acquire this spectral data for the most detailed examination yet of the atmosphere of a Jupiter-like planet beyond the solar system. 

"The most exciting part of this result is that we were able to make these observations of an exoplanet atmosphere with this level of detail, much more than I even imagined was possible," Konopacky said. "We have broken the light from the planet down to such a fine level of detail that the chemical fingerprints of the molecules in the atmosphere are breathtakingly sharp and distinct. This is important because it requires data of this quality to truly probe the makeup of a planetary atmosphere, and in turn, say something about how the planet formed."

Missing methane: a clue

The scientists detected water and carbon monoxide in the exoplanet's atmosphere, but not methane.

The lack of methane "tells us that there must be mixing between the different layers of the atmosphere, much like a lava lamp swirls material up and down," Konopacky said. "Since methane is a sensitive molecule, it can be destroyed when it gets mixed into the deeper, hotter parts of the atmosphere. This mixing tells us about the atmospheric conditions in young Jupiter-like planets."

In addition, although the researchers see a lot of water vapor in the atmosphere of HR 8799c, "we actually detect slightly less than we would have expected if the planet had the same composition as its host star," Konopacky said. "This tells us that the planet has a slightly elevated amount of carbon compared to oxygen." 

This high ratio of carbon to oxygen is a clue regarding the exoplanet's formation. The researchers suggest that grains of water ice condensed in the disc of matter surrounding HR 8799 that gave rise to the planets orbiting the star. Oxygen inside the ice depleted any other oxygen for the formation of HR 8799c.

"These ice grains stuck together to make bigger ice chunks, a few kilometers across, that kept colliding and building up the planet's solid core," Konopacky said. "The atmosphere came later — from gas that the planet attracted after it got big enough. By the time that happened, some of the ice grains were gone and the gas didn't have as much water in it."

How planets are born

These findings imply that a planet-building mechanism known as core accretion led to the formation of HR 8799c, "much in the same way we think the planets in our own solar system formed," Konopacky said. The exoplanet's core arose first, and the atmosphere came afterward.

"These results represent a first step in finding direct evidence about how planets form, which in general, is a difficult thing to do observationally," Konopacky said. "It is really exciting that we have these tantalizing suggestions that this extrasolar system that looks like our own solar system in so many ways may have formed in the same way."

Researchers are now tinkering with existing models of core accretion to see how planets might form via the process at great distances from their stars. For instance, there may be more matter at the outer edges of the protoplanetary discs of matter around stars that give rise to planets than before thought, or perhaps solid matter could stick together and form planetary cores easier or faster than previously suspected.

"By further refining the core accretion model of formation to explain the HR 8799 planets, we may be able to learn more about the formation of planetary systems in general, including our own solar system," Konopacky said.

"We would also like to discover more planets through direct imaging that can be studied at this level of detail," Konopacky added. "We work on a new instrument called the Gemini Planet Imager that is designed to do just this. It will arrive at the Gemini South Telescope in Chile this year, and discover new planets that are both smaller than the HR 8799 planets and closer to their parent star."

Konopacky and her colleagues Travis Barman, Bruce Macintosh and Christian Marois detailed their findings online March 14 in the journal Science. ( space.com )


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Extreme Earth Microbes Pave Way for Discovery of Alien Life


Extreme Earth Microbes Pave Way for Discovery of Alien LifeThe region beneath Earth's surface may be crawling with diverse organisms, and now researchers reveal the lives of just one group of bizarre beasties: methane-spewing microbes that hide out in the cracks of hot undersea volcanoes.

Called high-temperature methanogens, these microbes rely on the hydrogen and carbon dioxide in their superheated deep-sea vents for growth, excreting waste products like methane.

The possibility of past or present life on other worlds such as Mars, where the rover Curiosity has just set out to investigate whether the environment was ever fit for microbes, will become clearer by figuring out the extreme limits (or minimum requirements) for some organisms on Earth.

The research submarine Alvin reaches with its mechanical arm to a high-temperature black smoker at the Endeavour Segment, Juan de Fuca Ridge, to study methanogenic microbes.

"Evidence has built over the past 20 years that there's an incredible amount of biomass in the Earth's subsurface, in the crust and marine sediments, perhaps as much as all the plants and animals on the surface," microbiologist James Holden at the University of Massachusetts said in a statement. "We're interested in the microbes in the deep rock, and the best place to study them is at hydrothermal vents at undersea volcanoes. Warm water flows bring the nutrient and energy sources they need."

One way to figure out what's hidden beneath Earth's crust in extreme environments is to figure out the energy requirements of an organism and then see if various spots meet these thresholds for life. "We're really interested in the equivalent of, 'What is the size of your paycheck and what's the cost of living?'" Holden told LiveScience. "How much energy is available for microorganisms: the paycheck. And what's the lower threshold – they need this much energy to live in this environment."

To do this, the researchers collected methanogens from hydrothermal vents and tried growing them (along with commercially bought microbes) on different levels of hydrogen. From these experiments, they found the bare minimum of hydrogen that these microbes needed to survive (they all needed about the same concentrations).

Next, Holden and colleagues sent the deep submersible vehicle Alvin to test out the findings at two spots: the Axial volcano and the Endeavor segment, both observatory sites along an undersea mountain range well off the coast of Washington state and Oregon and about 1 to 1.5 miles (1.6 to 2.4 kilometers) below the surface of the Pacific Ocean.

Alvin collected samples from the sites' black smokers, where mineral-rich, superheated water ? up to 662 degrees Fahrenheit (350 degrees Celsius) ? spews out of Earth's crust through cracks in the seafloor, and it also took samples from surrounding, lower-temperature waters.

The hydrogen limits found in the lab held up in the field. At the Axial volcano site, where the scientists found hydrogen levels above the lab-determined threshold, they also found evidence of methanogenic microbes; at Endeavour, hydrogen levels were below the threshold, with evidence of methane-producers largely absent. However, they found heat-loving methanogens could survive by feeding on hydrogen produced by other extreme organisms living near the vent.

In addition to painting a more comprehensive picture of Earth's biodiversity today, the findings may reveal what life was like on early Earth, "where we think [life] was independent of sun and oxygen," Holden said.

His research also can be used beyond Earth, he says; the astrobiology community uses this sort of data to rule in or out the possibility of past extraterrestrial life on, say, Mars or the Jupiter moon Europa.

"How much energy is available and what's the 'cost of living' for these organisms, and could Mars have had enough energy to support this kind of life?" Holden said during a telephone interview.

The research, detailed this week in the journal Proceedings of the National Academy of Sciences, was supported by the National Science Foundation, NASA Astrobiology Institute and the National Oceanographic and Atmospheric Administration. ( LiveScience.com )


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New Zealand Volcano Eruption Seen from Space


New Zealand Volcano Eruption Seen from Space - The late-night eruption of New Zealand's Mount Tongariro volcano on Monday (Aug. 6) was spotted by a NASA satellite just an hour after it began.

The newly-released image, taken by the Suomi NPP satellite, shows the ash plume emanating from Tongariro at 12:55 a.m. New Zealand time on Aug. 7 (12:55 p.m. UTC Aug. 6). This was the volcano's first eruption in 115 years.

The eruption was a short-lived phreatic one, New Zealand volcano monitoring authorities said. hreatic eruptions are stream-driven eruptions that happen when water beneath or above the ground is heated up, potentially causing it to boil and "flash to steam," creating an explosion, according to the U.S. Geological Survey.

The ash plume from the eruption of New Zealand's Mount Tongariro volcano was spotted by NASA's Suomi NPP satellite at 12:55 a.m. New Zealand time on Aug. 7, 2012. 

The volcano lies in sparsely populated part of the North Island and no injuries were reported, according to a NASA statement.

Tongariro is 6,940 feet (1,978 meters) high and is part of the so-called "Pacific Ring of Fire" region known for its seismic activity and volcanism.

The eruption of the volcano sent ash at least 20,000 feet (6,100 m) into the air, according to the New Zealand Herald. Because ash plumes can be a danger to aircraft engines, some domestic flights were halted and other flights were re-routed, NASA said.

The potential danger makes detecting these plumes important, which is where satellites like Suomi NPP can come in. The satellite's Visible Infrared Imaging Radiometer Suite (VIIRS), which acquired the new image, is able to detect ash plumes lit by moonlight — a helpful trait during a nighttime eruption. VIIRS can also detect the thermal signature of such a plume closer to its source and lower in the atmosphere that many conventional methods can.

"Such information can give forecasters a heads-up in terms of changes in ash production and low-level wind shifts that may re-direct these hazardous plumes," Steven Miller of the Cooperative Institute for Research in the Atmosphere at Colorado State University said in the NASA statement.

The eruption activity seems to have subsided for now. Steam clouds have been seen near the volcano's Te M?ri craters, where the explosion originated.

Ash samples have been collected from the area and will be tested to see whether it is old rock blasted out by the explosion or new magma, which could suggest that magma is rising beneath the volcano, according to Erik Klemetti, an assistant professor of Geosciences at Denison University in Ohio and author of Wired's Eruptions Blog. Rising magma might mean that more eruptions could occur. No lava flows occurred from the eruption, though. ( LiveScience.com )


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Spooky! Quantum Action Is 10,000 Times Faster Than Light


Spooky! Quantum Action Is 10,000 Times Faster Than Light - How fast do quantum interactions happen? Faster than light, 10,000 times faster.

That's what a team of physicists led by Juan Yin at the University of Science and Technology of China in Shanghai found in an experiment involving entangled photons, or photons that remain intimately connected, even when separated by vast distances.They wanted to see what would happen if you tried assigning a speed to what Einstein called "spooky action at a distance."


Here, a false-color image of a laser beam showing a superposition of entangled photons spinning in opposite directions. 

They didn't find anything unexpected, but that wasn't the point: in physics, sometimes it's good to be sure. The group published their work on the ArXiv.org, a preprint server for physics papers.

All tangled up

Quantum physicists have long known that after two particles — photons, for example — interact, they sometimes become "entangled." This kind of experiment has been repeated many times, and involves taking two entangled photons and sending them to different places. Perhaps photon A goes to Los Angeles and photon B goes to Boston.

When photon A is observed, it has a certain polarization, perhaps "up." The other photon in Boston is always in the opposite polarization, "down." No matter what measurement is made of photon A, photon B will always be opposite. It is impossible to tell what the polarization will be before you measure it, but the entangled photons always seem to "know" the right state to be in, instantaneously.

As Chad Orzel, assistant professor of physics at Union College, explained, "It's as though you sent two cards to two different addresses. One might be the jack of diamonds and the other the ace of hearts. When you get the card at one address you know which one went to the other. Quantum mechanics is weird because until you open the envelope, saying which card it is doesn't have any meaning; it could be either one."

Speed of quantum interaction

This is what Albert Einstein called "spooky action at a distance." And the correlation between the photons' states seems to happen instantaneously. But what does "instantaneous" really mean? That's part of what the Chinese team wanted to look at.

So the researchers entangled two photons and sent them to two different stations about 10 miles (16 kilometers) apart. In their ArXiv paper, the scientists said that previous experiments had "locality loopholes," which is another way of saying that it's possible to explain the link between photons with something other than the "action at a distance."

The group measured the state of one photon and timed how long the entangled state took to show up in the other. They found that the slowest possible speed for quantum interactions is 10,000 times the speed of light — assuming your experiment is moving relatively slowly, at least relative to light beams.

Whereas the result may sound like a way to send faster-than-light messages, it isn't, really, because you can't know the state of the entangled photon pair before it's measured; so there's no way to control it and make the photon at the other end take on certain states and use it like a Morse code telegraph.

This type of experiment has been done before, notably by a European team, in 2008. So why do it again? Many physics experiments are performed to check more closely the values of constants used in equations, for instance, which enable more precise measurements in other areas.

Orzel said that even if it turned out that there was some small amount of time it takes for the state of a photon to change (meaning it's not instantaneous), it isn't clear that lag would mean much for quantum physics generally. That's because there are several interpretations for why quantum phenomena happen the way they do, and all explain the experimental results equally well. Physicists aren't even certain that there's an experiment one could do to tell the difference.

He added that it is extremely unlikely that anyone will ever get an "exact" value for the speed of such quantum interactions, and, in fact, modern physics prohibits that kind of finding in principle. But it is useful to see what the limits are — to clarify what we mean when we say "instantaneous."

"There's a certain strain of physics that people that will say it has to be instantaneous – in fact, if it is faster than light it must be instantaneous," Orzel said. "So if you can put a limit on it that is kind of cool." ( LiveScience.com ) 


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Massive meteorite crater found in Canadian Arctic


Massive meteorite crater found in Canadian Arctic - Researchers in Canada's western Arctic have found evidence of a crater that formed when a huge meteorite slammed into Earth millions of years ago.

Measuring about 15 miles (25 kilometers) across, the formation was named the Prince Albert impact crater after the peninsula where it was discovered. Researchers don't know exactly when it was created, but evidence suggests the crater is between 130 million and 350 million years old, according to a statement from the University of Saskatchewan.

http://t0.gstatic.com/images?q=tbn:ANd9GcS-Pwa4oQGds6oJNOzut7BxRc80ArCBAe-bckplNSRElUacnPFG

Meteors are fragments of asteroids or comets that enter Earth's atmosphere at high speeds; most are small, some as tiny as a grain of sand, so they disintegrate in the air, and only rarely are they large enough to make it to Earth's surface. When meteors slam into Earth, they are called meteorites.

A team of geologists spotted this newly identified meteorite crater while surveying the region for possible energy and mineral resources. They were initially intrigued by steeply tilted strata visible in river gorges and other features in the flat tundra of northwestern Victoria Island.

"Unless you recognized the telltale clues, you wouldn't know what you were looking at," researcher Brian Pratt explained in the statement. "You might see a bunch of broken rocks and wonder how they got there, but we found abundant shatter cones."

Shatter cones are surface features with distinctive wavy patterns that are known to be created only by the tremendous force of a meteorite impact or an underground nuclear explosion. What's more, Pratt said his map showed that the feature is circular, which is characteristic of impact craters.

"Impact craters like this give us clues into how the Earth's crust is recycled and the speed of erosion, and may be implicated in episodes of widespread extinction of animals in the geological past," Pratt said. "It's an exciting discovery."

There are about 180 known impact craters on Earth. Geologists think they would find countless more if plate shifting, volcanic activity and erosion didn't hide the evidence of most ancient impacts.

Earlier this summer, researchers in Greenland documented possibly the oldest and largest meteorite crater ever found on Earth. The crater, estimated to be 3 billion years old, currently measures about 62 miles (100 km) across. But the researchers believe its width before erosion was likely more than 310 miles (500 km) — much bigger than the largest visible crater, the 2-billion-year-old Vredefort crater in South Africa, which measures 186 miles (300 km) across. (


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